| 青海省3.2m地温场与年降水量、地震趋势的关系 |
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| 引用本文： | 孙武林.青海省3.2m地温场与年降水量、地震趋势的关系[J].高原地震,1997(1). |
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| 作者姓名： | 孙武林 |
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| 作者单位： | 青海省气象台!西宁，810001 |
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| 摘 要： | 通过对1980—1995年青海省3．2m地温距平场与年降水量距平％场、年地震释放总能量的相关分析，指出：若某地区地温异常偏高且干旱少雨，则未来该区可能发生地震。因3．2m地温变化缓慢，该结论具有一定的预报意义。
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| 关 键 词： | 地温场 降水量 地震 地温异常 |
THE RELATION BETWEEN 3.2m DEPTH GEOTHE-KM AL FIELD AND YEARLY PRECIPITATION' SEISMIC TENDECE IN QINGHAI PROVINCE |
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| Sun Wulin.THE RELATION BETWEEN 3.2m DEPTH GEOTHE-KM AL FIELD AND YEARLY PRECIPITATION'''' SEISMIC TENDECE IN QINGHAI PROVINCE[J].Plateau Earthquake Research,1997(1). |
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| Authors: | Sun Wulin |
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| Abstract: | The relation between the distance average of the 3. 2m depth geotemperature and me distance average field of yearly precipitation and yearly amount of seismic energy release is alialysed in this paper. The result shows that if it is drought with less raining and the temperature is extreamly high, the earthquake will occur in this area. Because the geotemperature of 3. 2mdepth changes slowly, the result has certain predictional significance. |
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| Keywords: | Geothermal field Precipitation Earthquake Geotemperature anomaly |
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